The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica

Abstract: Dissolved organic matter (DOM) comprises a significant pool of Earth's organic carbon that dwarfs the amount present in living aquatic organisms. The properties and reactivity of DOM are not well defined, and the evolution of autochthonous DOM from its precursor materials in freshwate...

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Main Author: Foreman, Christine
Format: Dataset
Language:unknown
Published: IEDA: US Antarctic Program Data Center 2014
Subjects:
Online Access:http://get.iedadata.org/metadata/iso/600104
id dataone:http://get.iedadata.org/metadata/iso/600104
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spelling dataone:http://get.iedadata.org/metadata/iso/600104 2024-10-03T18:45:37+00:00 The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica Foreman, Christine BEGINDATE: 2009-07-01T00:00:00Z ENDDATE: 2014-06-30T00:00:00Z 2014-01-01T00:00:00Z http://get.iedadata.org/metadata/iso/600104 unknown IEDA: US Antarctic Program Data Center Antarctic Organisms and Ecosystems Microbiology Biology Glaciology Antarctica Glaciers/Ice Sheet Biosphere Cryosphere US Antarctic Program Data Center (USAP-DC) Dataset 2014 dataone:urn:node:IEDA_USAP 2024-10-03T18:12:02Z Abstract: Dissolved organic matter (DOM) comprises a significant pool of Earth's organic carbon that dwarfs the amount present in living aquatic organisms. The properties and reactivity of DOM are not well defined, and the evolution of autochthonous DOM from its precursor materials in freshwater has not been observed. Recent sampling of a supraglacial stream formed on the Cotton Glacier in the Transantarctic Mountains revealed DOM that more closely resembles an assemblage of recognizable precursor organic compounds, based upon its UV-VIS and fluorescence spectra. It is suggested that the DOM from this water evolved over time to resemble materials present in marine and many inland surface waters. The transient nature of the system i.e., it reforms seasonally, also prevents any accumulation of the refractory DOM present in most surface waters. Thus, the Cotton Glacier provides us with a unique environment to study the formation of DOM from precursor materials. An interdisciplinary team will study the biogeochemistry of this progenitor DOM and how microbes modify it. By focusing on the chemical composition of the DOM as it shifts from precursor material to the more humified fractions, the investigators will relate this transition to bioavailability, enzymatic activity, community composition and microbial growth efficiency. This project will support education at all levels, K-12, high school, undergraduate, graduate and post-doc and will increase participation by under-represented groups in science. Towards these goals, the investigators have established relationships with girls' schools and Native American programs. Additional outreach will be carried out in coordination with PolarTREC, PolarPalooza, and if possible, an Antarctic Artist and Writer. Dataset Antarc* Antarctic Antarctica Ice Sheet IEDA: US Antarctic Program Data Center (via DataONE) Antarctic Transantarctic Mountains Cotton Glacier ENVELOPE(161.667,161.667,-77.117,-77.117)
institution Open Polar
collection IEDA: US Antarctic Program Data Center (via DataONE)
op_collection_id dataone:urn:node:IEDA_USAP
language unknown
topic Antarctic Organisms and Ecosystems
Microbiology
Biology
Glaciology
Antarctica
Glaciers/Ice Sheet
Biosphere
Cryosphere
US Antarctic Program Data Center (USAP-DC)
spellingShingle Antarctic Organisms and Ecosystems
Microbiology
Biology
Glaciology
Antarctica
Glaciers/Ice Sheet
Biosphere
Cryosphere
US Antarctic Program Data Center (USAP-DC)
Foreman, Christine
The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica
topic_facet Antarctic Organisms and Ecosystems
Microbiology
Biology
Glaciology
Antarctica
Glaciers/Ice Sheet
Biosphere
Cryosphere
US Antarctic Program Data Center (USAP-DC)
description Abstract: Dissolved organic matter (DOM) comprises a significant pool of Earth's organic carbon that dwarfs the amount present in living aquatic organisms. The properties and reactivity of DOM are not well defined, and the evolution of autochthonous DOM from its precursor materials in freshwater has not been observed. Recent sampling of a supraglacial stream formed on the Cotton Glacier in the Transantarctic Mountains revealed DOM that more closely resembles an assemblage of recognizable precursor organic compounds, based upon its UV-VIS and fluorescence spectra. It is suggested that the DOM from this water evolved over time to resemble materials present in marine and many inland surface waters. The transient nature of the system i.e., it reforms seasonally, also prevents any accumulation of the refractory DOM present in most surface waters. Thus, the Cotton Glacier provides us with a unique environment to study the formation of DOM from precursor materials. An interdisciplinary team will study the biogeochemistry of this progenitor DOM and how microbes modify it. By focusing on the chemical composition of the DOM as it shifts from precursor material to the more humified fractions, the investigators will relate this transition to bioavailability, enzymatic activity, community composition and microbial growth efficiency. This project will support education at all levels, K-12, high school, undergraduate, graduate and post-doc and will increase participation by under-represented groups in science. Towards these goals, the investigators have established relationships with girls' schools and Native American programs. Additional outreach will be carried out in coordination with PolarTREC, PolarPalooza, and if possible, an Antarctic Artist and Writer.
format Dataset
author Foreman, Christine
author_facet Foreman, Christine
author_sort Foreman, Christine
title The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica
title_short The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica
title_full The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica
title_fullStr The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica
title_full_unstemmed The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica
title_sort biogeochemical evolution of dissolved organic matter in a fluvial system on the cotton glacier, antarctica
publisher IEDA: US Antarctic Program Data Center
publishDate 2014
url http://get.iedadata.org/metadata/iso/600104
op_coverage BEGINDATE: 2009-07-01T00:00:00Z ENDDATE: 2014-06-30T00:00:00Z
long_lat ENVELOPE(161.667,161.667,-77.117,-77.117)
geographic Antarctic
Transantarctic Mountains
Cotton Glacier
geographic_facet Antarctic
Transantarctic Mountains
Cotton Glacier
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
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